Comparison of Costello Geomagnetic Activity Index Model and JHU/APL Models for Kp Prediction
By: David Marchese Mentors: Douglas Biesecker Christopher Balch
Comparison of Costello Geomagnetic Activity Index Model and JHU/APL - - PowerPoint PPT Presentation
Comparison of Costello Geomagnetic Activity Index Model and JHU/APL Models for Kp Prediction By: David Marchese Mentors: Douglas Biesecker Christopher Balch Outline Background Kp Prediction Costello Geomagnetic Activity Index
By: David Marchese Mentors: Douglas Biesecker Christopher Balch
Background Kp Prediction Costello Geomagnetic Activity Index Model
Validation Studies
Research Results JHU/APL Models Conclusions
horizontal components of Earth’s magnetic field caused by solar particle radiation
using observations from 13 subauroral magnetometer stations
Range from 0 to 9 in a
scale of thirds
Kp value of 0
corresponds to the quietest conditions
Kp value of 9
corresponds to the most disturbed conditions
Quasi-logarithmic
scale
ap index ranges from 0
to 400 and represents the Kp value converted to a linear scale in nT
from the Boulder-NOAA Magnetometer
6, and 7 or greater are expected
and 9
Official Kp index published
“Nowcast” Kp algorithm
Derived using data from 9
Calculated by the United
response of Kp to solar wind data
speed, IMF magnitude, and Bz
minutes
Space weather forecasters need to know how reliable
Several validation studies have been done on the
Results are not complimentary Important to determine the reasons for discrepancies
1978 to February 16, 1980 (ISEE-3)
between 0 and 7
values
underprediction
Study performed by members of the Space Environment Center.
(IMP-8, Wind, ACE)
interpolating between points to match 15 minute time granularity
underpredict high Kp values
underprediction
Study performed by Wing et al.
during solar minimum years
from July 1, 1998 until June 18, 2007
2006
uninterrupted since 1932
Time granularity
Model predictions are made approximately every 15
Official Kp values are calculated once every 3 hours
Solution
Time-tag each of the official Kp values at the beginning of
deviation in length
showing the upper and lower quartiles
underprediction
underprediction
During solar
maximum external influences dominate activity in the magnetosphere
During solar
minimum internal dynamics are responsible for fluctuations in magnetic field strength
Solar Maximum Solar Minimum
Costello model appears to predict low Kp values slightly better during solar
maximum years
Solar Maximum Solar Minimum
Figures show the distribution of official Kp values for Costello predictions
corresponding to NOAA warnings Expected Kp of 6 (G2 storm) Expected Kp of 7 or greater (G3 or higher storm)
Figures show the distribution of official Kp values for Costello predictions
corresponding to NOAA warnings Expected Kp of 4 Expected Kp of 5 (G1 storm)
APL Model 1
Inputs nowcast Kp and solar
wind parameters
Predicts Kp 1 hour ahead
APL Model 2
Same inputs as APL Model 1 Predicts Kp 4 hours ahead
APL Model 3
Inputs solar wind parameters Predicts Kp 1 hour ahead
Inputs nowcast Kp and solar
Predicts Kp 1 hour ahead Correlation coefficient = 0.92
underprediction
Inputs nowcast Kp and solar
Predicts Kp 4 hours ahead Correlation coefficient = 0.79
underprediction
Inputs solar wind parameters Predicts Kp 1 hour ahead Correlation coefficient = 0.84
underprediction
Interpolated Official Kp No Interpolation Interpolated Official Kp
Interpolation of official Kp
When no interpolation is
Similar skew may be
No Interpolation
APL models installed Code edited to run on a
Models successfully produce
Real-time data plots were not
Modifications to run models
dependency
JHU/APL models perform significantly better than the Costello model
Detman, T., and J. A. Joselyn (1999), Real-time Kp predictions
Wing, S., J. R. Johnson, J. Jen, C.-I. Meng, D. G. Sibeck, K.
sd-www.jhuapl.edu/UPOS/ www.gfz-potsdam.de www.n3kl.org www.ngdc.noaa.gov www.sec.noaa.gov
Douglas Biesecker Christopher Balch
Simon Wing Janice Schofield